At a convergent boundary.
if seafloor is created at a divergent boundary then it must be the opposite (at a convergent boundary) where is being destroyed.
The sea floor is destroyed in subduction zones, where one tectonic plate is pushed beneath another. This process is responsible for the destruction of oceanic crust and the formation of deep ocean trenches.
The youngest seafloor is located at mid-ocean ridges, which are divergent plate boundaries where tectonic plates move apart. As new oceanic crust is formed through seafloor spreading, it pushes older crust away from the ridge, making the seafloor at mid-ocean ridges the youngest on Earth.
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
Seafloor spreading occurs at the boundary between tectonic plates because of the divergent movement of these plates. As the plates move apart, magma rises from the mantle to fill the gap, solidifying as it cools and creating new seafloor. This process is instrumental in the formation of mid-ocean ridges and plays a key role in the theory of plate tectonics.
The sea floor is destroyed in subduction zones, where one tectonic plate is pushed beneath another. This process is responsible for the destruction of oceanic crust and the formation of deep ocean trenches.
Seafloor is created at divergent plate boundaries called the mid-ocean ridges.
Divergent Plate Boundary. (Seafloor Spreading).
At a divergent boundary, land is gained. Ocean ridges are prominent at divergent plate boundaries. Ocean ridges are areas of seafloor spreading. Seafloor spreading occurs as upwelling magma rises to the surface. This upwelling magma hardens and forms new seafloor.
A divergent boundary creates seafloor spreading. At these boundaries, tectonic plates move apart, allowing magma to rise from below the Earth's surface and create new crust at the mid-ocean ridges.
The youngest seafloor is located at mid-ocean ridges, which are divergent plate boundaries where tectonic plates move apart. As new oceanic crust is formed through seafloor spreading, it pushes older crust away from the ridge, making the seafloor at mid-ocean ridges the youngest on Earth.
recessive plate boundary
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
Seafloor spreading occurs at the boundary between tectonic plates because of the divergent movement of these plates. As the plates move apart, magma rises from the mantle to fill the gap, solidifying as it cools and creating new seafloor. This process is instrumental in the formation of mid-ocean ridges and plays a key role in the theory of plate tectonics.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
it's neither created or destroyed
A conservative boundary, also known as a transform boundary, is where crust is neither created nor destroyed. This type of boundary occurs when two tectonic plates slide past each other horizontally.